trying to explore new probably mineralized areas depending on the previous knowledge and data acquired from a mineralized ones around them.
See these papers which are available on request on the RG server:
DILL, H.G. (2020) A geological and mineralogical review of clay mineral deposits and phyllosilicate ore guides in Central Europe - A function of geodynamics and climate change.- Ore Geology Reviews 119 (on-line)
DILL, H.G. (2017) An overview of the pegmatitic landscape from the pole to the equator – Applied geomorphology and ore guides.- Ore Geology Reviews 91: 795 – 823.
DILL, H.G. (2017) Residual clay deposits on basement rocks: The impact of climate and the geological setting on supergene argillitization in the Bohemian Massif (Central Europe) and across the globe.- Earth Sciences Reviews 165: 1-58.
DILL, H.G. (2016) Kaolin: soil, rock and ore From the mineral to the magmatic, sedimentary, and metamorphic environments.- Earth Sciences Reviews 161: 16-129.
DILL, H.G., WEBER, B. and BOTZ, R. (2013) Metalliferous duricrusts (“orecretes”) - markers of weathering: A mineralogical and climatic-geomorphological approach to supergene Pb-Zn- Cu-Sb-P mineralization on different parent materials.- Neues Jahrbuch für Mineralogie Abhandlungen, 190: 123-195
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DILL, H.G., GERDES, A. and WEBER, B. (2010) Age and mineralogy of supergene uranium minerals - tools to unravel geomorphological and palaeohydrological processes in granitic terrains (Bohemian Massif, SE Germany).- Geomorphology, 117: 44-65.
There is an over generalization when considering the concept of Climatic Geomorphology. There are other factors which play important roles in geomorphic processes and landform development such as the geological formation, vegetal cover, structural stability etc. Hence, climate should not be singled out either directly or indirectly without taking into cognizance the role played by other factors.
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